innlánsforma

Innlandsforma is a term used in geology to describe landforms that are created by processes occurring far from oceanic coastlines. These formations are distinct from coastal landforms shaped by wave action, tides, and marine erosion. Inland processes include those driven by internal geological forces like tectonics and volcanism, as well as external forces such as weathering, erosion by rivers and glaciers, and the deposition of sediments.

Common examples of innlandsforma include mountain ranges, plateaus, valleys carved by rivers or glaciers, deserts, and plains. Volcanic cones and calderas are also innlandsforma, as are features resulting from tectonic activity such as fault scarps and rift valleys. The scale of innlandsforma can vary significantly, from small erosional remnants to vast continental landscapes. Their development is typically a slow process, influenced by climate, rock type, and the underlying geological structure. Studying innlandsforma helps geologists understand the Earth's history, its dynamic processes, and the distribution of resources.